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首页> 外文期刊>Erdkunde >DYNAMICS AND DRIVING FORCES OF TREELINE FLUCTUATION AND REGENERATION IN CENTRAL NORWAY DURING THE PAST DECADES
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DYNAMICS AND DRIVING FORCES OF TREELINE FLUCTUATION AND REGENERATION IN CENTRAL NORWAY DURING THE PAST DECADES

机译:过去十年间中部挪威海岸线波动与再生的动力学和驱动力

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摘要

The aim of this study was to analyse recent tteeline fluctuations in central Norway to estimate the influence of land use change and climatic change during the past decades. Four study areas were chosen along steep oceanic-continental gradients in central Norway, representing different climatic regions. The analysis was performed using a combination of landscape-ecological, dendroecological, remote sensing and human-geographical methods. Treeline alterations were analysed by correlating climate change signals and spatial land use changes. All study sites showed a spatial expansion of forest fragments within the alpine tteeline ecotone but little regeneration above the recent tteeline. We found that intensive historical land use by logging and grazing had decreased the tteeline at the beginning of the 20th century. Recent regeneration was found, mainly due to land use extensification. Climate analysis indicated warmer and moister conditions over the past decades. We found that these changes were restricted to the winter months, only. Furthermore, regeneration occurred on plots formerly disturbed by heavy grazing pressure or cryoturbation. Climatic change during the past decades had no effect on tteeline fluctuations. The most decisive driving forces for tteeline fluctuation and regeneration were changes of land use intensity. On the one hand, grazing pressure was the initial trigger for the expansion of forest fragments within the tteeline ecotone. On the other, high grazing intensity combined with other land use practises caused stable stages of depressed tteelines.
机译:这项研究的目的是分析挪威中部最近的三通线波动,以估计过去几十年来土地利用变化和气候变化的影响。沿着挪威中部陡峭的海洋-大陆梯度选择了四个研究区域,分别代表不同的气候区域。分析是结合景观生态学,树状生态学,遥感和人文地理方法进行的。通过关联气候变化信号和空间土地利用变化来分析林线变化。所有研究地点均显示了高山tteeline过渡带内森林碎片的空间扩展,但在最近的tteeline之上几乎没有再生。我们发现,在20世纪初,伐木和放牧对土地的密集使用减少了tteeline。发现最近的更新,主要是由于土地利用的扩大化。气候分析表明,过去几十年来气候变暖和潮湿。我们发现这些更改仅限于冬季。此外,在原先受到高放牧压力或低温扰动干扰的地块上发生了再生。在过去的几十年中,气候变化对三通的波动没有影响。 Tteeline波动和再生的决定性驱动力是土地利用强度的变化。一方面,放牧压力是tteeline过渡带内森林碎片扩张的最初诱因。另一方面,高放牧强度与其他土地利用做法相结合,导致了tteeline处于稳定阶段。

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